He observed, also, that while some species of the fossils contained in
these rocks were common to both sides of the Atlantic, the majority were
different; thus disproving the statement which at that time was often
made--namely, that in the rocks older than the Carboniferous system the
fossil fauna in different parts of the globe was almost everywhere the
same, and showing that, "however close the present analogy of forms may
be, there is evidence of the same law of variation in space as now
prevails in the living creation."
Lyell made a thorough study of the Falls of Niagara, to which he paid a
second visit before his return to England. The first view of these
Falls, like the first sight of a great snow-clad peak, is one of those
epochs of life of which the memory can never fade. It stirred Lyell to
an unwonted enthusiasm. At the first view, from a distance of about
three miles, with not a house in sight--it would be impossible, we
think, to find such a spot now; "nothing but the greenwood, the falling
water, and the white foam"--he thought the falls "more beautiful but
less grand" than he had expected; but, after spending some days in the
neighbourhood, now watching the river sweeping onwards to its final
plunge, here in the turmoil of the rapids, there in its gliding, so
smooth but so irresistible; now gazing at that mighty wall of 'shattered
chrysoprase' and rainbow-tinted spray, which floats up like the steam of
Etna; now looking down from the brink of the crags below the fall upon
those rapids, where the billows of green water roll and plunge like the
waves of the ocean, he "at last learned by degrees to comprehend the
wonders of the scene, and to feel its full magnificence."
Public-domain text, read in full here on John Shaqi.
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